| 松桃地区南华纪锰矿研究现状及进展综述 |
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| 引用本文： | 陈袆,王中群.松桃地区南华纪锰矿研究现状及进展综述[J].贵州地质,2010,27(2):95-99. |
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| 作者姓名： | 陈袆 王中群 |
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| 作者单位： | 贵州大学资源与环境工程学院,贵州贵阳,550003 |
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| 摘 要： | 黔东地区地处扬子板块东南缘与江南造山带的结合部位。受新元古代Rod inia超大陆裂解作用,在华南形成了新元古代被动陆缘裂谷盆地,呈北东—北北东向展布的断裂系控制了该区南华纪早期菱锰矿沉积盆地的分布。本文就该区锰矿床分布特征及成因研究进展方面进行简述,最后提出寻找"大塘坡式"锰矿的标志:冷泉碳酸盐岩。
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| 关 键 词： | 松桃地区锰矿 分布特征 研究进展 标志 |
Research condition and process of manganese deposit of Nanhua period in Songtao area |
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| CHEN Yi,WANG Zhong-qun.Research condition and process of manganese deposit of Nanhua period in Songtao area[J].Guizhou Geology,2010,27(2):95-99. |
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| Authors: | CHEN Yi WANG Zhong-qun |
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| Institution: | (Resource and Environment School of Guizhou University,Guiyang 550003,Guizhou,China) |
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| Abstract: | East Guizhou is located in the combined position of Yangtze plate and Jiangnan orogenic belt.Because of the Rodinia pyrolysis process in Neoproterozoic Era,passive continental rift basin of Neoproterozoic Era formed in south China,the NE-NNE distributed fault series controlled the distribution of phosphorus manganese deposit in early Nanhua period.In this paper,the distribution characters and formation research of phosphorus manganese deposit in this area are simply narrated,finally it＇s suggested to find the criteria of ＇Datangpo＇ manganese deposit： coal spring carbonate rock. |
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| Keywords: | manganese deposit in Songtao distribution character research condition criteria |
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